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100			_aForke, Sven _951397
245			_aSources of laminated sediments in the northeastern Arabian Sea off Pakistan and implications for sediment transport mechanisms during the late Holocene/
260			_bSage, _c2019.
300			_aVol 29, issue 1, 2019 : (130-144 p.).
520			_aLaminated sediments of the continental slope off the Makran coast in the northern Arabian Sea are well-known climate archives and record productivity, as well as supply of material from land. Here, we studied sediment core 275KL off Pakistan in concert with sediment trap, dust and river samples in order to characterize and quantify land-derived material deposited in varves and event layers. We analysed grain sizes, mineral assemblages, bulk components and stable isotopes (δ13C, δ18O) of carbonates. In winter, enhanced river discharge is the main source of lithogenic matter contributing the major amounts to the total annual sedimentation of the northern Arabian Sea. During the late summer season, lithogenic matter accumulation is slightly enhanced, probably carried along with the south-eastward blowing Levar winds from the Balochistan and the Sistan Basins and the summer monsoon discharge maximum of perennial streams. C/N ratios and stable carbon and oxygen isotopes could not be used to distinguish between organic matter produced on land and in the ocean, whereas stable carbon and oxygen isotope ratios of carbonates suggest that sedimentation of event layers is dominated by direct inputs from land. Catastrophic denudation and storm events occur on average once every 50 years and lead to sedimentation rates that exceed the mean annual sedimentations of 983 g m−2 yr−1 by 6 to 10 times. Nevertheless, due to their rare occurrence, they contributed only 7% to the total sedimentation during the last ca. 5000 years. End-member modelling of grain sizes in accordance with lithogenic matter accumulation rates and event layer frequencies showed that arid conditions prevailed between 4000 and 5000 a BP while more humid conditions commenced around 2000 ka BP in accordance with the Pacific ENSO record.
650			_a Arabian Sea, _951398
650			_aENSO, _951399
650			_a erosion, _950967
650			_a grain size, _951400
650			_a Holocene climate, _951401
650			_a laminated sediments, _951402
650			_a lithogenic matter, _951403
650			_awestern disturbances _951404
700			_aRixen, Tim _951405
700			_aBurdanowitz, Nicole _951406
700			_aLückge, Andreas _951407
700			_aRamaswamy, Venkitasubramani _951408
700			_aMunz, Philipp _951409
700			_aWilhelms-Dick, Dorothee _951410
700			_aVogt, Christoph _951411
700			_aKasten Sabine _951412
700			_aGaye, Birgit _951413
773	0		_012756 _916504 _dLondon: Sage Publication Ltd, 2019. _tHolocene/ _x09596836
856			_uhttps://doi.org/10.1177/0959683618804627
942			_2ddc _cART
999			_c12767 _d12767